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Updated: Jun 21, 2025

06:55
Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
Published on: August 5, 2016
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Los cristales antiguos muestran que la tectónica de placas comenzó temprano
Resumen
Los circones antiguos indican que la subducción de la corteza oceánica comenzó hace aproximadamente 4 mil millones de años. Este proceso geológico temprano proporciona información sobre la Tierra
Área de la Ciencia:
- Geología
- Geocronología
- Tectónica de placas
Sus antecedentes:
- Los circones son minerales robustos que preservan la evidencia de las primeras condiciones de la Tierra.
- Las investigaciones anteriores se han centrado en períodos posteriores de iniciación de la subducción.
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